A link is provided below for more information.
Continental plates are made of basalt, while oceanic plates are made of granite.
Oceanic plates are primarily made up of basaltic rock while continental plates are primarily made of granitic rock. Basalt is denser than granite which allows oceanic plates to subduct beneath continental plates.
All major plates contain both continental and oceanic crust except for the Pacific and Nazca plates.
when two plates collide they form trenches.
In plate tectonics, a convergent boundary, also known as a destructive plate boundary (because of subduction), is an actively deforming region where two (or more) tectonic plates or fragments of lithosphere move toward one another and collide. As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries. When two plates move towards one another, they form either a subduction zone or a continental collision. This depends on the nature of the plates involved. In a subduction zone, the subducting plate, which is normally a plate with oceanic crust, moves beneath the other plate, which can be made of either oceanic or continental crust. During collisions between two continental plates, large mountain ranges, such as the Himalayas are formed.
A mountain gets made
Continental crust is made primarily of granite.
Sometimes
plates There are continental plates (thick and made of granite) and oceanic plates (thin and made of basalt).
yes
Sometimes
Continental plates are made of granite
The two types of tectonic plates are continental and oceanic.
Granite.
it creates a lava monster
The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere. The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere.
Continental Crust is the layer of rocks that forms the continents and continental shelves. It is mostly made of granite or granitic rock.
The majority of the continental plates is composed of SiO2, silicon dioxide, much of it in the form of the feldspar, mica, and quartz minerals.